Exoplanetology: Exoplanets & Exomoons

Volatile-rich Sub-Neptunes as Hydrothermal Worlds: The Case of K2-18 b

By Keith Cowing
Status Report
astro-ph.EP
September 11, 2024
Filed under , , , , , , , , , , , ,
Volatile-rich Sub-Neptunes as Hydrothermal Worlds: The Case of K2-18 b
Possible conceptual structures for K2-18 b that are explored previously (Hu 2021; Hu et al. 2021; Tsai et al. 2021; Yu et al. 2021; Madhusudhan et al. 2023b; Shorttle et al. 2024; Wogan et al. 2024) and in this work. — astro-ph.EP

Temperate exoplanets between the sizes of Earth and Neptune, known as “sub-Neptunes”, have emerged as intriguing targets for astrobiology.

It is unknown whether these planets resemble Earth-like terrestrial worlds with a habitable surface, Neptune-like giant planets with deep atmospheres and no habitable surface, or something exotic in between. Recent JWST transmission spectroscopy observations of the canonical sub-Neptune K2-18 b revealed ~1% CH4, ~1% CO2, and a non-detection of CO in the atmosphere.

While previous studies have proposed that the observed atmospheric composition could help constrain the lower atmosphere conditions and determine the interior structure of sub-Neptunes like K2-18 b, the possible interactions between the atmosphere and a hot, supercritical water ocean at its base remain unexplored.

In this work, we investigate whether a global supercritical water ocean, resembling a planetary-scale hydrothermal system, can explain these observations on K2-18 b-like sub-Neptunes through equilibrium aqueous geochemical calculations.

We find that the observed atmospheric CH4/CO2 ratio implies a minimum ocean temperature of ~715 K, whereas the corresponding CO/CO2 ratio allows ocean temperatures up to ~1060 K. These results indicate that a global supercritical water ocean on K2-18 b is plausible.

While life cannot survive in this ocean, this work represents the first step towards understanding how a global supercritical water ocean may influence observable atmospheric characteristics on volatile-rich sub-Neptunes.

Future observations with better constrained NH3 and CO mixing ratios could further help distinguish between possible interior compositions of K2-18 b.

Cindy N. Luu, Xinting Yu, Christopher R. Glein, Hamish Innes, Artyom Aguichine, Joshua Krissansen-Totton, Julianne I. Moses, Shang-Min Tsai, Xi Zhang, Ngoc Truong, Jonathan J. Fortney

Comments: 15 pages, 5 figures, 1 table
Subjects: Earth and Planetary Astrophysics (astro-ph.EP)
Cite as: arXiv:2409.06258 [astro-ph.EP] (or arXiv:2409.06258v1 [astro-ph.EP] for this version)
https://doi.org/10.48550/arXiv.2409.06258
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Submission history
From: Xinting Yu
[v1] Tue, 10 Sep 2024 07:00:42 UTC (2,350 KB)
https://arxiv.org/abs/2409.06258
Astrobiology

Explorers Club Fellow, ex-NASA Space Station Payload manager/space biologist, Away Teams, Journalist, Lapsed climber, Synaesthete, Na’Vi-Jedi-Freman-Buddhist-mix, ASL, Devon Island and Everest Base Camp veteran, (he/him) 🖖🏻